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- W2444582279 abstract "Two different tectonic models have been proposed for the thick Eocene depocenter located along the northeastern margin of the Maracaibo basin, Venezuela. The first model proposes that the depocenter is a foreland basin controlled by southwestward-directed overthrusting during late Paleocene-middle Eocene collision between the Caribbean and South American plates. The second model proposes that the northeast sedimentary wedge was controlled by a large tear fault, or lateral ramp, separating SE-directed, but independently moving, thrust sheets. Regional seismic lines reveal the structure of the Paleogene depocenter in the northeastern area of the Maracaibo basin. The Burro Negro fault forms a line of separation between shallow to outer shelf, less deformed rocks to the SW from deep marine highly deformed rocks to the NE. Configuration of the basin and faults mapped on regional-scale 2D seismic lines tied to wells supports a tear, or lateralramp fault origin, which allowed SE migration of the thrust front east of the Maracaibo basin." @default.
- W2444582279 created "2016-06-24" @default.
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- W2444582279 date "2003-01-01" @default.
- W2444582279 modified "2023-09-26" @default.
- W2444582279 title "Paleogene Depocenter along the Northeast Margin of the Maracaibo Basin: Structure along an Exhumed, Eocene Age Lateral Ramp Fault in the Maracaibo Basin, Western Venezuela*" @default.
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